Noun:

সংঘাত শিলা,

clastic rocks's Usage Examples:

There are three peat layers, interspersed with fine-grained clastic rocks, and they have been studied with pollen and foraminifera analyses.

longer than 4 metres) produced on the ground and typically formed by clastic rocks or similarly durable elements of the landscape, such as stones, stone.

diameter of individual grains of sediment, or the lithified particles in clastic rocks.

from the Greek: πῦρ, meaning fire; and κλαστός, meaning broken) are clastic rocks composed of rock fragments produced and ejected by explosive volcanic.

the deposition of fluvio-deltaic sediments which consists mainly of clastic rocks (claystones, shales, siltstones, sandstones, conglomerates) interstratified.

It is a sequence of fine grained clastic rocks (claystones, mudstones, siltstones) interbedded with freshwater carbonates.

Paleogene rocks from the early Cenozoic include volcanic and marine clastic rocks, associated with high rates of erosion.

geology, maturity describes the composition and texture of grains in clastic rocks, most typically sandstones, resulting from different amounts of sediment.

Carboniferous to Lower Jurassic volcanic rocks, carbonate rocks, coarse clastic rocks and small amounts of ultramafic rock, chert and argillite.

Early Paleozoic rocks include clastic rocks with calcareous intercalations near the Pannonian region and along the.

rocks, Cambrian mafic volcanics, Ordovician limestone and Silurian clastic rocks were all deformed and metamorphosed.

Igneous clastic rocks can be divided into two classes: Broken, fragmental rocks associated.

Paleogene led to the formation of rift basins in which thick sequences of clastic rocks were deposited that are exposed at the eastern end of the island in.

Early Paleozoic granites followed by a gap in the Aptian and pelagic clastic rocks from the Cretaceous.

Kvamshesten Basin is a sedimentary basin containing coarse continental clastic rocks of Devonian age.

includes shallow marine Permian and Triassic platform carbonates and clastic rocks.

SEDEX deposits are hosted largely by clastic rocks deposited in intracontinental rifts or failed rift basins and passive.

consists of quartz sand, multicolour clay, and fine-grained mellow clastic rocks, that has yielded remnants of fish and flora.

Synonyms:

disintegrative;

Antonyms:

integrative; tie-on;